Geochemistry of hydrothermal tourmaline from IOCG occurrences in the Great Bear magmatic zone: Implications for fluid source(s) and fluid composition evolution

Author:

Kelly C.J.,Davis W.J.,Potter E.G.,Corriveau L.

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference91 articles.

1. Acosta-Góngora, P., Gleeson, S.A., Ootes, L., Jackson, V.A., Lee, M., Samson, I., 2011. Preliminary observations on the IOCG mineralogy at the Damp, Fab, and Nori showings and Terra-Norex mines, Great Bear magmatic zone. Northwest Territories Geological Survey, NWT Open File Report 2011-001.

2. Trace element geochemistry of magnetite and its relationship to Cu-Bi-Co-Au-Ag-U-W mineralization in the Great Bear magmatic zone, NWT, Canada;Acosta-Góngora;Econ. Geol.,2014

3. Gold refining by bismuth melts in the iron oxide-dominated NICO Au-Co-Bi (±Cu±W) deposit, NWT, Canada;Acosta-Góngora;Econ. Geol.,2015

4. Genesis of the Paleoproterozoic NICO iron-oxide-cobalt-gold-bismuth deposit, Northwest Territories, Canada: evidence from isotope geochemistry and fluid inclusions;Acosta-Góngora;Precambr. Res.,2015

5. Origin of sulfur and crustal recycling of copper in polymetallic (Cu-Au-Co-Bi-U ± Ag) iron-oxide-dominated systems of the Great Bear Magmatic Zone, NWT, Canada;Acosta-Góngora;Mineral. Depos.,2018

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